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    • Late Quaternary Sedimentation and Slope Failure Events on the Costa Rican Margin 

      Nath, B.N.; Yatheesh, V.; Yazing, A.K.; Prabhu, S.R.; Borker, A.; Pandey, D.K.; KameshRaju, K.A. (Springer, Cham, 2020)
      The Costa Rican margin is an erosional convergent margin formed by subduction of the Cocos Plate under the Caribbean Plate along the Middle America Trench. The Integrated Ocean Drilling Program (IODP) Expedition 334 was ...